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Mid-Pleistocene transition in glacial cycles explained by declining CO(2) and regolith removal
Variations in Earth’s orbit pace the glacial-interglacial cycles of the Quaternary, but the mechanisms that transform regional and seasonal variations in solar insolation into glacial-interglacial cycles are still elusive. Here, we present transient simulations of coevolution of climate, ice sheets,...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2019
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6447376/ https://www.ncbi.nlm.nih.gov/pubmed/30949580 http://dx.doi.org/10.1126/sciadv.aav7337 |